The Atlantic Monthly, volume 12, No. 69, July, 1863

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what didthe Silurian and Devonian epochs add to these earliest tracts of dry landin the Old World? and where do we find the coal basins which show us thesites of her Carboniferous forests? Since the relation between the epochsof comparative tranquillity and the successive upheavals has been socarefully traced in Europe, I will endeavor, while giving a sketch of thatearly European world, to point out, at the same time, the connection ofthe different systems of upheaval with the successive strati...fied deposits, without, however, entering into such details as must necessarily becometechnical and tedious.
In the European ocean of the Azoic epoch we find five islands ofconsiderable size. The largest of these is at the North. Scandinavia hadeven then almost her present outlines; for Norway, Sweden, Finland, andLapland, all of which are chiefly granitic in character, were among thefirst lands to be raised. Between Sweden and Norway, there is, however, still a large tract of land under water, forming an extensive lake or alarge inland sea in the heart of the country.


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